Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8081123 | Journal of Environmental Radioactivity | 2016 | 9 Pages |
Abstract
The concentrations of 137Cs in the air, which were divided into coarse (>1.1 μm Ï) and fine (<1.1 μm Ï) fractions of particulate matter (PM), were measured from October 2012 to December 2014 in an area evacuated after the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident. Total atmospheric 137Cs concentrations showed a clear seasonal variation, with high concentrations during summer and autumn related to the dominant easterly wind blowing from the highly radioactivity contaminated area. This seasonal peak was dominated by 137Cs in the coarse PM fraction. The 137Cs specific activity (massic 137Cs concentration) in the coarse PM was also found to increase significantly in summer, whereas that in the fine PM showed no variability during the year. These results show that coarse and fine 137Cs-bearing PM have different origins and behaviors in the resuspension process. The seasonal variation in atmospheric 137Cs concentration was well correlated with the mean 137Cs surface contamination (deposition density) around the observation site weighted by the frequency of wind direction, indicating that the atmospheric 137Cs concentration in the observation site was explained by the distribution of the 137Cs surface contamination and the frequency of different wind directions. We introduced a resuspension factor corrected for wind direction, consisting of the ratio of the atmospheric 137Cs concentration to the weighted mean 137Cs surface contamination, which evaluated the intensity of resuspension better than the conventional resuspension factor. This ratio ranged from 5.7 Ã 10â11 to 8.6 Ã 10â10 mâ1 and gradually decreased during the study period.
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Nuclear Energy and Engineering
Authors
Shinya Ochiai, Hidenao Hasegawa, Hideki Kakiuchi, Naofumi Akata, Shinji Ueda, Shinji Tokonami, Shun'ichi Hisamatsu,